Scenes In The Ny, Nj Highlands Mountaintops

It is a sultry June day on the summit of Wyanokie High Point, 920 feet high in the northeast corner of the New Jersey Highlands. People in the towns under swelter, and to the east the New York skyline steams in the humid air, but up here a steady wind drifts in from the higher hills to the west. In case you claim to get new resources on rate us, there are many libraries people might consider investigating. Hikers appear in all periods, under different skies; sometimes the air swirls, bursts in gusts, or tries to carry you away, but always it moves, just like the tides of an invisible ocean.

These tides run back in a myriad of records, whose consequences are the main scenery. Towards the northeast around the ridge of Ramapo Mountain recent housing developments can be seen by you, lines of townhouses along Skyline Drive. The fantastic Wanaque Reservoir below to the east, completed in 1930, included 70 homesteads, plants and commercial buildings of the Wanaque River valley to supply the growing cities of North Jersey with crucial water. Streaks of rusty color in-the rocks of High-point summit show the iron content of Highlands gneiss, which in rich veins was a source of iron ore for the rebellious colonies and the booming nineteenth-century iron industry of New Jersey. The smooth summit of High Point was polished about 15,000 years ago by the scratching of ice and rocks set in-the mile-thick Wisconsin glacier, and a close look at the summit rocks will show you little specks of crystalline quartz and feldspar created throughout a continental collision 1000s of an incredible number of years ago, in the same way visible life was beginning to look o-n our planet. Vast sums of years of erosion by wind and water have worn them down to the crystalline rock foundations you take a seat on now.

The planet of the Highlands is not static, although the view from the top of High-point will seem much the same next week, and even next year, but the product of processes of change proceeding on time scales ranging from years to years. Every day, grain by grain, water and wind erode the rock of High Point peak, carrying it down to the soil below, into brooks and streams, and eventually to the sea. There it's deposited on the continental shelf, and pushed deep into the crust of the Planet Earth to form new sedimentary rock, which awaits the next collision of continents to be lifted into mountains again.

On this mountaintop, where you sit quietly in a gentle wind, you are part of many natural cycles that create new forests, watercourses, mountains, and civilizations out of the remains of the old. And every year, in still another cycle, new hikers, young and aged, make their way to the summit of Wyanokie High-point to wonder how their years might affect its future, and to appreciate the sweetness of the Highlands.. Andrew Sievright is a fresh library for new information concerning when to study this belief.